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Callister - An introduction - 8th edition

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20.5 <strong>An</strong>tiferromagnetism and Ferrimagnetism • 809<br />

Figure 20.8 Schematic representation of antiparallel<br />

alignment of spin magnetic moments for antiferromagnetic<br />

manganese oxide.<br />

Mn 2+<br />

0 2–<br />

20.5 ANTIFERROMAGNETISM AND<br />

FERRIMAGNETISM<br />

<strong>An</strong>tiferromagnetism<br />

antiferromagnetism<br />

This phenomenon of magnetic moment coupling between adjacent atoms or ions<br />

occurs in materials other than those that are ferromagnetic. In one such group, this<br />

coupling results in an antiparallel alignment; the alignment of the spin moments of<br />

neighboring atoms or ions in exactly opposite directions is termed antiferromagnetism.<br />

Manganese oxide (MnO) is one material that displays this behavior. Manganese<br />

oxide is a ceramic material that is ionic in character, having both Mn 2 and<br />

O 2 ions. No net magnetic moment is associated with the O 2 ions, because there is<br />

a total cancellation of both spin and orbital moments. However, the Mn 2 ions possess<br />

a net magnetic moment that is predominantly of spin origin. These Mn 2 ions<br />

are arrayed in the crystal structure such that the moments of adjacent ions are antiparallel.<br />

This arrangement is represented schematically in Figure 20.8. Obviously,<br />

the opposing magnetic moments cancel one another, and, as a consequence, the<br />

solid as a whole possesses no net magnetic moment.<br />

ferrimagnetism<br />

Ferrimagnetism<br />

Some ceramics also exhibit a permanent magnetization, termed ferrimagnetism. The<br />

macroscopic magnetic characteristics of ferromagnets and ferrimagnets are similar;<br />

the distinction lies in the source of the net magnetic moments. The principles of ferrimagnetism<br />

are illustrated with the cubic ferrites. 2 These ionic materials may be<br />

represented by the chemical formula MFe 2 O 4 , in which M represents any one of<br />

several metallic elements. The prototype ferrite is Fe 3 O 4 , the mineral magnetite,<br />

sometimes called lodestone.<br />

The formula for Fe 3 O 4 may be written as Fe 2 O 2 –(Fe 3 ) 2 (O 2 ) 3 , in which the<br />

Fe ions exist in both 2 and 3 valence states in the ratio of 1:2. A net spin magnetic<br />

moment exists for each Fe 2 and Fe 3 ion, which corresponds to 4 and 5 Bohr<br />

magnetons, respectively, for the two ion types. Furthermore, the O 2 ions are magnetically<br />

neutral. There are antiparallel spin-coupling interactions between the Fe<br />

ions, similar in character to antiferromagnetism. However, the net ferrimagnetic<br />

moment arises from the incomplete cancellation of spin moments.<br />

Cubic ferrites have the inverse spinel crystal structure, which is cubic in symmetry,<br />

and similar to the spinel structure (Section 12.2). (A unit cell for this inverse<br />

spinel structure is shown on the front cover of the book. Red spheres represent<br />

ferrite<br />

2<br />

Ferrite in the magnetic sense should not be confused with the ferrite -iron discussed in<br />

Section 9.18; in the remainder of this chapter, the term ferrite implies the magnetic ceramic.

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